This research aims to document the lateral/vertical relationships between turbidite channelized deposits and lobe deposits, which are recurrent depositional elements in deep-water marine systems.Deliverables and expected results are the following:

- to develop a comprehensive facies scheme and to provide a detailed reconstruction of the stratigraphic architecture of these coarse-grained slope systems;

- to place all these slope systems within an accurate sequence stratigraphic framework through the breakdown of the deep-water successions into vertical sequence of hierarchical architectural elements and genetic units.

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